2016
DOI: 10.1127/metz/2015/0583
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Decadal predictability of regional-scale peak winds over Europe using the Earth System Model of the Max-Planck-Institute for Meteorology

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Cited by 7 publications
(11 citation statements)
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“…These findings are in line with Haas et al (2015), who evaluated the decadal predictability of regional peak winds in the MiKlip ensemble baseline1 and also found highest skill scores for short lead times. The enhanced skill scores for higher percentiles are also consistent with results by Haas et al (2015), who showed, for example, that the enhanced storminess over Central Europe in the early nineties (leading to enhanced peak winds at the surface) could be identified in the baseline1 hindcasts. Such skill is not found for lower percentiles (Haas et al, 2015; their figure 7).…”
Section: Summary and Discussionsupporting
confidence: 89%
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“…These findings are in line with Haas et al (2015), who evaluated the decadal predictability of regional peak winds in the MiKlip ensemble baseline1 and also found highest skill scores for short lead times. The enhanced skill scores for higher percentiles are also consistent with results by Haas et al (2015), who showed, for example, that the enhanced storminess over Central Europe in the early nineties (leading to enhanced peak winds at the surface) could be identified in the baseline1 hindcasts. Such skill is not found for lower percentiles (Haas et al, 2015; their figure 7).…”
Section: Summary and Discussionsupporting
confidence: 89%
“…The enhanced skill scores for higher percentiles are also consistent with results by Haas et al (2015), who showed, for example, that the enhanced storminess over Central Europe in the early nineties (leading to enhanced peak winds at the surface) could be identified in the baseline1 hindcasts. Such skill is not found for lower percentiles (Haas et al, 2015; their figure 7).…”
Section: Summary and Discussionsupporting
confidence: 89%
See 2 more Smart Citations
“…We evaluate the performance of both the global MPI-ESM and the regional CCLM hindcasts with the following datasets. For temperature and precipitation, we consider the observational dataset E-OBS (Haylock et al, 2008) As no gridded dataset is available for wind, a CCLM simulation forced with boundary conditions from ERA40 and ERA-Interim is employed as verification dataset for wind speed. For this reanalysis-driven simulation, CCLM is applied in the same model set-up as for the regionalization of the global hindcast ensemble (see above).…”
Section: Datamentioning
confidence: 99%